Because there's no way to directly
study deep mantle rocks, Panero and Pigott are probing the question with high - pressure physics experiments and computer calculations.
Not exact matches
Scientists
studying volcanic hotspots have strong evidence of this, finding high helium - 3 relative to helium - 4 in some plumes, the upwellings from Earth's
deep mantle.
The Hawaii research relies on a new seismic technique for detecting aligned flows of rock that has yet to be verified, says marine geophysicist Cecily Wolfe of the Woods Hole Oceanographic Institution in Massachusetts and the Carnegie Institution of Washington, D.C.. However, the Iceland
study is «very clear and compelling,» she says, and consistent with a
deep mantle origin for the plume.
The
study shows that the carbon cycle extends
deep into
mantle, possibly all the way down to the core -
mantle boundary, with billion year storage times.
Now a recent
study, led by Arizona State University's School of Earth and Space Exploration Associate Professor Dan Shim, has re-created in the laboratory the conditions found
deep in the Earth, and used this to discover an important property of the dominant mineral in Earth's
mantle, a region lying far below our feet.
The larger and rarer rough diamonds analyzed in this
study — those measuring around a centimeter or more on their longest side — formed
deeper within the
mantle, taking scientists» understanding of the
mantle to new depths.
More perplexing still, seismic
studies have shown no evidence that ocean crust is being subducted — thrust down into the hot
mantle underlying the trench — which is the process that results in quakes at other
deep - sea trenches.
The finding, in combination with evidence from previous
studies, suggests that these molten regions
deep below, near the core -
mantle boundary of the Earth, may cause basaltic ocean island chains to form along the surface.
«For the first time we could obtain images of the
deeper crustal structure in the region where the Walvis Ridge joins the African continent, in order to
study the impact of a
mantle plume» explains Trond Ryberg from GFZ.
According to the NASA press release, the
study «adds evidence that a geothermal heat source called a
mantle plume lies
deep below Antarctic Marie Byrd Land, explaining some of the melting that creates lakes and rivers under the ice sheet.»
A new NASA
study adds evidence that a geothermal heat source called a
mantle plume lies
deep below Antarctica's Marie Byrd Land, explaining some of the melting that creates lakes and rivers under the ice sheet.